29 citations as recorded by crossref.

1. Morphology of Ionospheric Sporadic E Layer Intensity Based on COSMIC Occultation Data in the Midlatitude and Low‐Latitude Regions J. Niu et al. 10.1029/2019JA026828
2. Interhemispheric transport of metallic ions within ionospheric sporadic <i>E</i> layers by the lower thermospheric meridional circulation B. Yu et al. 10.5194/acp-21-4219-2021
3. Quarterdiurnal signature in sporadic E occurrence rates and comparison with neutral wind shear C. Jacobi et al. 10.5194/angeo-37-273-2019
4. A Case Study of the Daytime Intense Radar Backscatter and Strong Ionospheric Scintillation Related to the Low‐Latitude E‐Region Irregularities G. Chen et al. 10.1029/2019JA027532
5. Global Empirical Model of Sporadic-E Occurrence Rates E. Parsch et al. 10.3389/fspas.2024.1434367
6. Longitudinal Structure in the Altitude of the Sporadic E Observed by COSMIC in Low-Latitudes Z. Liu et al. 10.3390/rs13224714
7. Characterizing global equatorial sporadic-E layers through COSMIC GNSS radio occultation measurements A. Seif & S. Panda 10.1007/s10509-024-04326-2
8. Relationship Between Wavenumber 4 Pattern of Sporadic E Layer Intensity and Eastward Propagating Diurnal Tide With Zonal Wavenumber 3 in Low Latitude Region J. Niu 10.1029/2020JA028985
9. Statistical study of medium-scale traveling ionospheric disturbances in low-latitude ionosphere using an automatic algorithm P. Cheng et al. 10.1186/s40623-021-01432-1
10. The Characteristics of Summer Descending Sporadic E Layer Observed With the Ionosondes in the China Region L. Qiu et al. 10.1029/2020JA028729
11. Detection and localization of F-layer ionospheric irregularities with the back-propagation method along the radio occultation ray path V. Ludwig-Barbosa et al. 10.5194/amt-16-1849-2023
12. Estimation Model of Global Ionospheric Irregularities: An Artificial Intelligence Approach P. Tian et al. 10.1029/2022SW003160
13. Wavenumber‐4 Patterns of the Sporadic E Over the Middle‐ and Low‐Latitudes Z. Liu et al. 10.1029/2021JA029238
14. Evidence of anti-correlation between sporadic (Es) layers occurrence and solar activity observed at low latitudes over the Brazilian sector P. Fontes et al. 10.1016/j.asr.2023.09.040
15. Examining the Wind Shear Theory of Sporadic E With ICON/MIGHTI Winds and COSMIC‐2 Radio Occultation Data Y. Yamazaki et al. 10.1029/2021GL096202
16. Global ionosonde and GPS radio occultation sporadic-E intensity and height comparison J. Gooch et al. 10.1016/j.jastp.2020.105200
17. Global Structure and Seasonal Variations of the Tidal Amplitude in Sporadic‐E Layer Q. Tang et al. 10.1029/2022JA030711
18. An Empirical Model of the Sporadic E Layer Intensity Based on COSMIC Radio Occultation Observations J. Niu & H. Fang 10.1029/2022SW003280
19. Sporadic E layer characteristics at equatorial latitudes as observed by GNSS radio occultation measurements C. Arras et al. 10.1186/s40623-022-01718-y
20. Migrating and nonmigrating tidal signatures in sporadic E layer occurrence rates C. Jacobi et al. 10.5194/ars-20-85-2023
21. Disturbances in Sporadic‐E During the Great Solar Eclipse of August 21, 2017 G. Chen et al. 10.1029/2020JA028986
22. A Signature of 27 day Solar Rotation in the Concentration of Metallic Ions within the Terrestrial Ionosphere B. Yu et al. 10.3847/1538-4357/ac0886
23. Tidal wind shear observed by meteor radar and comparison with sporadic E occurrence rates based on GPS radio occultation observations C. Jacobi & C. Arras 10.5194/ars-17-213-2019
24. Derivation of global ionospheric Sporadic E critical frequency ( f o Es) data from the amplitude variations in GPS/GNSS radio occultations B. Yu et al. 10.1098/rsos.200320
25. Deriving Ionospheric Sporadic E Intensity From FORMOSAT‐3/COSMIC and FY‐3C Radio Occultation Measurements T. Hu et al. 10.1029/2022SW003214
26. Comparison of global morphologies of vertical ion convergence and sporadic E occurrence rate L. Qiu et al. 10.1016/j.asr.2019.02.024
27. An Empirical Model of the Ionospheric Sporadic E Layer Based on GNSS Radio Occultation Data B. Yu et al. 10.1029/2022SW003113
28. Statistical Characteristics of the Low‐Latitude E‐Region Irregularities Observed by the HCOPAR in South China C. Yan et al. 10.1029/2021JA029972
29. Using GNSS radio occultation data to derive critical frequencies of the ionospheric sporadic E layer in real time B. Yu et al. 10.1007/s10291-020-01050-6